PREDICTIONS OF CRUSTAL DEFORMATION CAUSED BY CHANGING POLAR ICE ON A VISCOELASTIC EARTH

Geophysical surveys - Tập 18 - Trang 303-312 - 1997
John Wahr1, Dazhong Han2
1Department of Physics and Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, USA
2Department of Physics, University of Colorado, Boulder

Tóm tắt

Changes in polar ice could cause vertical crustal motion of up to several mm yr-1 along the edge of the Greenland and Antarctic ice caps. Measurements of the uplift could help constrain the changing ice volumes. The problem is complicated by the Earth's visco-elastic response to past loading, including the Late Pleistocene deglaciation. A method is described for removing these visco-elastic effects, by using simultaneous measurements of vertical motion and surface gravity. A linear combination of these two measurement types can be formed which is relatively independent of visco-elastic effects, and which can be interpreted in terms of present-day fluctuations in ice.

Tài liệu tham khảo

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